We have scored the climate risk of the 39.288 buildings in Las Palmas de Gran Canaria using Cadastre data, satellite imagery and climate projections, and added it up by area, street and watercourse. The clearest change comes at night: from 45 to 84 tropical nights a year by 2050.
Level of the highest hazard in each 250 m area by 2050: flooding, heat, wildfire, wind or ground movement.
Position among the 8.217 municipalities: further right means more risk. These are figures for the municipality as a whole, the same for everyone; they may differ from those for the typical building. Compare with others →
It comes from matching each building with its neighbourhood, its street, the nearest watercourse and its surroundings.
These are 6.893 buildings right next to vegetation that can burn. Of these, 30 are blocks of flats with 1.449 homes, where evacuation is harder.
Proximity to woodland and to burnt areas (ESA WorldCover, EFFIS). It does not measure the state of the vegetation or any firebreaks.
In a typical building in Las Palmas de Gran Canaria, nights when the temperature stays at or above 20 °C would rise from 45 a year (1991-2020) to about 84 by 2050. For this reason, 100 % of homes would be at a high or very high level.
Median of the buildings. Intermediate-to-high emissions scenario (SSP3-7.0).
That is 1 % of homes. The extreme sea level in a 100-year storm reaches 2,34 m today and 2,61 m by 2050.
Ground elevation at the building (IGN digital terrain model). Being low-lying does not mean it will flood: that depends on the beach, sea defences and drainage.
Schools whose surroundings are at least 1 °C hotter than the municipal median in summer. They are the first candidates for shade and tree-lined playgrounds.
Ground surface temperature (Landsat) around the building closest to the OpenStreetMap point.
Along Barranco Guiniguada (9,3 km within the municipality, dry most of the year) there is no official mapped flood zone, but there are 306 homes less than 50 m from the watercourse.
Having no official map does not mean it cannot overflow: watercourses that are dry most of the year are the ones that cause the most surprises in a storm.
The 164.373 homes in Las Palmas de Gran Canaria by the level of their building. Tap a hazard to see it on the map.
The same data for all 8.217 municipalities in Spain. Choose what to compare with: municipalities of a similar size, the province, the region or the whole of Spain.
Compared with the 67 municipalities with more than 100.000 inhabitants. The bar shows where Las Palmas de Gran Canaria stands: further right means more risk.
| Indicator | Las Palmas de Gran Canaria | Group median | Position |
|---|---|---|---|
| Tropical nights a year, today | 32 nights | 18 nights | higher than 61 % of them |
| Tropical nights a year, 2050 | 81 nights | 60 nights | higher than 64 % of them |
| Average summer maximum, 2050 | 25,2 °C | 31,4 °C | lower than 84 % of them |
| Night-time heat island | 0,7 °C | 1,2 °C | lower than 78 % of them |
| Flood-prone area (100-year) | 0,0% | 3,9% | lower than 92 % of them |
| Area burnt 2016-2026 | 0,0% | 0,0% | lower than 72 % of them |
| Water stress 2050 (0-5) | 2,8 | 4,9 | lower than 79 % of them |
| Maximum 50-year gust | 31 m/s | 30 m/s | higher than 62 % of them |
| Ground movement | −1,5 mm/yr | −1,0 mm/yr | sinking faster than 93 % of them |
| Population aged 65 or over | 21% | 20% | higher than 57 % of them |
Compared with the 34 municipalities in Las Palmas province. The bar shows where Las Palmas de Gran Canaria stands: further right means more risk.
| Indicator | Las Palmas de Gran Canaria | Group median | Position |
|---|---|---|---|
| Tropical nights a year, today | 32 nights | 64 nights | lower than 81 % of them |
| Tropical nights a year, 2050 | 81 nights | 126 nights | lower than 66 % of them |
| Average summer maximum, 2050 | 25,2 °C | 26,2 °C | lower than 75 % of them |
| Night-time heat island | 0,7 °C | 0,2 °C | higher than 85 % of them |
| Flood-prone area (100-year) | 0,0% | 0,0% | higher than 50 % of them |
| Area burnt 2016-2026 | 0,0% | 0,0% | lower than 72 % of them |
| Water stress 2050 (0-5) | 2,8 | 2,8 | higher than 50 % of them |
| Maximum 50-year gust | 31 m/s | 28 m/s | higher than 75 % of them |
| Ground movement | −1,5 mm/yr | −1,3 mm/yr | sinking faster than 72 % of them |
| Population aged 65 or over | 21% | 18% | higher than 76 % of them |
Compared with the 88 municipalities in the Canary Islands. The bar shows where Las Palmas de Gran Canaria stands: further right means more risk.
| Indicator | Las Palmas de Gran Canaria | Group median | Position |
|---|---|---|---|
| Tropical nights a year, today | 32 nights | 41 nights | lower than 56 % of them |
| Tropical nights a year, 2050 | 81 nights | 78 nights | higher than 52 % of them |
| Average summer maximum, 2050 | 25,2 °C | 25,1 °C | higher than 52 % of them |
| Night-time heat island | 0,7 °C | 0,5 °C | higher than 61 % of them |
| Flood-prone area (100-year) | 0,0% | 0,0% | higher than 50 % of them |
| Area burnt 2016-2026 | 0,0% | 0,1% | lower than 75 % of them |
| Water stress 2050 (0-5) | 2,8 | 2,8 | higher than 50 % of them |
| Maximum 50-year gust | 31 m/s | 29 m/s | higher than 60 % of them |
| Ground movement | −1,5 mm/yr | −1,3 mm/yr | sinking faster than 64 % of them |
| Population aged 65 or over | 21% | 20% | higher than 60 % of them |
Compared with the 8.217 municipalities in Spain. The bar shows where Las Palmas de Gran Canaria stands: further right means more risk.
| Indicator | Las Palmas de Gran Canaria | Group median | Position |
|---|---|---|---|
| Tropical nights a year, today | 32 nights | 0 nights | higher than 92 % of them |
| Tropical nights a year, 2050 | 81 nights | 8 nights | higher than 93 % of them |
| Average summer maximum, 2050 | 25,2 °C | 32,4 °C | lower than 94 % of them |
| Night-time heat island | 0,7 °C | 0,1 °C | higher than 84 % of them |
| Flood-prone area (100-year) | 0,0% | 0,6% | lower than 80 % of them |
| Area burnt 2016-2026 | 0,0% | 0,0% | lower than 64 % of them |
| Water stress 2050 (0-5) | 2,8 | 4,6 | lower than 84 % of them |
| Maximum 50-year gust | 31 m/s | 31 m/s | higher than 51 % of them |
| Ground movement | −1,5 mm/yr | −0,4 mm/yr | sinking faster than 92 % of them |
| Population aged 65 or over | 21% | 28% | lower than 77 % of them |
Values for the municipality as a whole (median over built-up land). The position is the percentage of municipalities in the group with a lower value: it is not a probability of damage. 2050 = SSP3-7.0 scenario.
Semicolon-separated tables with a decimal comma, ready to open in a spreadsheet or a GIS (areas include longitude and latitude).
What this is and what it is not. It is a guide-only analysis made with public data and models, with the same rules for every municipality. It does not replace official maps, a technical study or emergency plans. For your own building, look up its report.
Building by building. We have scored the 39.288 Cadastre buildings in Las Palmas de Gran Canaria with the same rules as each building’s report on Mi Riesgo Climático, from 0 to 100 for each hazard: low (up to 25), medium (up to 50), high (up to 75) and very high.
Aggregates only. To protect each owner, no individual building appears here: only 250 m areas with at least 3 buildings, and neighbourhoods and streets with at least 60 homes.
Wildfire and flooding. Wildfire counts proximity to woodland or scrubland of at least 100 ha (not urban parks or tree-lined streets). For flooding, besides the official flood zones, a building that was inside a real flood observed by satellite (Copernicus EMS, such as the 2024 DANA storm) is at least at high level.
2050. Average for 2041-2070 under an intermediate-to-high emissions scenario (SSP3-7.0). Tropical nights and heat change with the climate; flooding, wildfire, wind and ground movement are shown with current data when there is no projection.
Rivers and streams. Named watercourses from OpenStreetMap. We count the homes less than 50 and 100 m from the watercourse and, separately, how many of them are in an official flood zone (SNCZI). Being close does not mean they will flood, and having no official zone does not mean they cannot.
Neighbourhoods and streets. Neighbourhoods and districts from OpenStreetMap; streets according to the Cadastre address. The street heat index combines tropical nights in 2050 (35 %), heat island (30 %), lack of trees (20 %) and buildings from before 1980 (15 %).
Sources. Cadastre (buildings and addresses); ERA5 + CHELSA/CMIP6 MPI-ESM1-2-HR and AdapteCCa (tropical nights and temperature); Landsat 8/9 and MODIS (heat island); ESA WorldCover and EFFIS (wildfire); MITECO SNCZI (flood zones); JRC (coast); ERA5 + Global Wind Atlas (wind); Copernicus EGMS (ground movement); WRI Aqueduct (water); INE (population); OpenStreetMap, © contributors, ODbL (streets, neighbourhoods, rivers and facilities).